Lecture: Chapter 23 - Biogeochemical Cycles Flashcards

1
Q

Biogeochemistry

A

The study of the physical, chemical and biological factors that influence the movement and transformation of elements.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Nutrient Cycles

A

There are about 100 elements
Approximately 40 are required by organisms
They cycle in the biosphere

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

The most important chemical elements

A

Carbon
Nitrogen
Phosporus
Sulfur

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Biogeochemical cycles

A

Inorganic (nonliving) - Biotic (living)

Elemetns are mostly moved in aqueous solution
Each cycle has a reservoir (atmosphere, ocean, sediments, rock, etc)

Some cycles are more perfect than others. Perfect is in the direction of very rapid transfer of the element to the environment followed by very rapid removal by organisms.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

How do nutrients enter ecosystems?

A

Through the chemical breakdown of minerals in rocks or through fixation of atmospheric gases

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Two basic biogeochemical cycles

A

Sedimentary / Solid (2.8% of living matter)
26 elements
The solid cycles are less “perfect”

Gaseous (97.2% of living matter)
4 elements : Carbon, hydrogen, oxygen, nitrogen
CHON

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Solid cycle

A

All nutrients are ultimately derived from abiotic sources; minerals in rocks and gases in the atmosphere

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Weathering

A

Elements are released from rock minerals by weathering physical and chemical breakdown of rocks

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Atmosphere

A

The atmosphere si the ultimate source of carbon and nitrogen for ecosytems

  • Carbon is taken up as CO2 by autrophs through photosynthesis and fixed into organic compounds
  • The atmosphere is 78% nitrogen, in the form of N2, which cannot be used by most organisms because of the energy required to break the triple covalent bond
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Nitrogen fixation

A

The process of converting N2 to a biologically useful form

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Pools

A

Total amount of a nutrient in a component of the ecosystem

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Mean residence time (turnover rate)

A

Amount of time on average that a molecule spends in the pool

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Where do freshwater and marine ecosytems receive nutrient inputs

A

Freshwater and marine ecosytems recieve nutrient inputs from terrestrial ecosytems

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Nutrients in aquatic ecosystems: Lakes

A

receive nutrients from stream water, atmospheric deposition, fixation and terrestrial litter.

  • phosphorus is usually the limiting nutrient in lakes
  • Detritus is decomposed int he water column and sediments, providing internal nutrient input
  • Nutrients are progressively lost as detritus is deposited in the lake sediments
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Carbon cycle

A

Closely linked to energy flow

the largest carbon pool is the ocean

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Net Ecosystem Production

A

Production available for accumulation of C/energy witihin the ecosystem

NEP = GPP - (RA+RH+L+D)

17
Q

Rate of Carbon cycle through the ecosytem determined by

A
  • Rate of primary productivity
  • Rate of decomposition

Both of these processes are influenced by climate

  • temperature
  • precipitation

Fastest cycling is in the hot and humid tropics

18
Q

Nitrogen cycle: an atmospheric cycle

A

The largest nitrogen pool is the atmosphere

The nitrogen cycle is a relatively perfect, self-regulating cycle with a large gaseous reservoir – the atmosphere, which is 78% N

Bacteria are responsible for key steps in the N cycle

The average resident time of fixed N in the biosphere is thought to be about 625 years while for P it is thousands of years.

19
Q

Nitrification

A

NH3 and NH4+ are converted to NO3- by chemoautotrophic bacteria, in aerobic conditions. It occurs mainly in terrestrial systems. NO3- tends to be more available to plants than other forms of nitrogen

20
Q

Denitrification

A

Some bacteria use NO3- as an electron acceptor, converting it into N2 and N20, in anoxic conditions

21
Q

Routes of N uptake

A

Uptake of N2 from atmosphere (very costly energetically)
- N fixtaion: high energy fixation, biological

Uptake of mineral nitrogen from soil

  • Ammonium (NH4+) : released by decomposition, created by deposition, affected by cation exchanged capacity
  • Nitrate (NO3): deposition, nitrification
22
Q

Factors affecting N release

A

Decomposition rate influenced by

  • water
  • temperature
  • litter quality
  • soil biota
23
Q

Human activity in N release

A

Human activity greatly increased the amount of N entering the biosphere through agricultural and industrial practices

24
Q

Sources of nitrate: nitrogen deposition

A

NOx emitted by fossil fuel burning

Some falls as dry deposition

Falls as wet acidic precipitation

25
Q

Nitrogen loss

A

Leaching

  • nitrate is primary form that is lost from ecosystems
  • Does not adhere to soils

Fire - volitilization of organic nitrogen

Dentrificiation
- Transformation of nitrate to N2
Requires: lack of oxygen, nitrate

26
Q

Phosophorus cycle

A

Solid chemical, essential nutrient that moves in sedimentary cycle, which is less perfect than gas cycles.

  • vital components of cells in organisms. Biological uses of phosphate: nucleic acids
  • P almost always present as phosphate PO4
  • Rock is the only source